← Part IV: EM Waves
Chapter 11

Electromagnetic Waves in Vacuum

Plane waves, polarization, energy, momentum, and radiation pressure.

11.1 Plane Wave Solutions

The simplest solution to the wave equation is the monochromatic plane wave. For a wave traveling in the $+\hat{z}$ direction:

$$\tilde{\mathbf{E}} = \tilde{E}_0 e^{i(kz - \omega t)}\hat{x}, \qquad \tilde{\mathbf{B}} = \frac{\tilde{E}_0}{c} e^{i(kz-\omega t)}\hat{y}$$

with the dispersion relation $\omega = ck$, $k = 2\pi/\lambda$. Key properties:

  • Transverse: $\mathbf{E}$ and $\mathbf{B}$ are both perpendicular to the propagation direction $\hat{k}$.
  • Mutual perpendicularity: $\mathbf{E} \perp \mathbf{B}$.
  • Amplitude ratio: $|\mathbf{B}| = |\mathbf{E}|/c$.
  • Phase relation: $\mathbf{E}$ and $\mathbf{B}$ are in phase.

Derivation: Electromagnetic Wave Equation in Vacuum

Starting from Maxwell's equations in vacuum (no charges, no currents):

Step 1: Write Maxwell's equations in vacuum

$$\nabla \cdot \mathbf{E} = 0, \quad \nabla \cdot \mathbf{B} = 0$$

$$\nabla \times \mathbf{E} = -\frac{\partial \mathbf{B}}{\partial t}, \quad \nabla \times \mathbf{B} = \mu_0\epsilon_0\frac{\partial \mathbf{E}}{\partial t}$$

Step 2: Take the curl of Faraday's law

$$\nabla \times (\nabla \times \mathbf{E}) = \nabla \times \left(-\frac{\partial \mathbf{B}}{\partial t}\right) = -\frac{\partial}{\partial t}(\nabla \times \mathbf{B})$$

Step 3: Apply the vector identity on the left side

$$\nabla \times (\nabla \times \mathbf{E}) = \nabla(\nabla \cdot \mathbf{E}) - \nabla^2\mathbf{E} = -\nabla^2\mathbf{E}$$

since $\nabla \cdot \mathbf{E} = 0$ in vacuum (Gauss's law with no charges).

Step 4: Substitute Ampere-Maxwell law on the right side

$$-\frac{\partial}{\partial t}(\nabla \times \mathbf{B}) = -\frac{\partial}{\partial t}\left(\mu_0\epsilon_0\frac{\partial \mathbf{E}}{\partial t}\right) = -\mu_0\epsilon_0\frac{\partial^2 \mathbf{E}}{\partial t^2}$$

Step 5: Combine to get the wave equation

$$\nabla^2\mathbf{E} = \mu_0\epsilon_0\frac{\partial^2 \mathbf{E}}{\partial t^2}$$

This is the electromagnetic wave equation. Comparing with the standard wave equation $\nabla^2 f = \frac{1}{v^2}\frac{\partial^2 f}{\partial t^2}$, we identify:

$$v = \frac{1}{\sqrt{\mu_0\epsilon_0}} = c = 2.998 \times 10^8 \text{ m/s}$$

Step 6: Identical equation for B

Taking the curl of Ampere-Maxwell law and using the same procedure yields:

$$\nabla^2\mathbf{B} = \mu_0\epsilon_0\frac{\partial^2 \mathbf{B}}{\partial t^2}$$

Both $\mathbf{E}$ and $\mathbf{B}$ satisfy the same wave equation and travel at the same speed $c$.

Derivation: Plane Wave Solution and Dispersion Relation

Starting from the wave equation, we seek a monochromatic plane wave solution propagating in the $\hat{z}$ direction.

Step 1: Propose a plane wave ansatz

$$\mathbf{E}(z,t) = E_0\cos(kz - \omega t + \phi)\,\hat{x}$$

where $k$ is the wave number, $\omega$ is the angular frequency, and $\phi$ is a phase constant.

Step 2: Compute the spatial derivatives

$$\nabla^2\mathbf{E} = \frac{\partial^2 E_x}{\partial z^2}\,\hat{x} = -k^2 E_0\cos(kz - \omega t + \phi)\,\hat{x} = -k^2\mathbf{E}$$

Step 3: Compute the time derivatives

$$\frac{\partial^2\mathbf{E}}{\partial t^2} = -\omega^2 E_0\cos(kz - \omega t + \phi)\,\hat{x} = -\omega^2\mathbf{E}$$

Step 4: Substitute into the wave equation

$$-k^2\mathbf{E} = \mu_0\epsilon_0(-\omega^2\mathbf{E}) \implies k^2 = \mu_0\epsilon_0\,\omega^2$$

Step 5: Obtain the dispersion relation

$$\omega = \frac{k}{\sqrt{\mu_0\epsilon_0}} = ck$$

This is a linear dispersion relation, meaning EM waves in vacuum are non-dispersive: all frequencies travel at the same speed $c$.

Step 6: Relate wavelength, frequency, and wave number

$$k = \frac{2\pi}{\lambda}, \quad \omega = 2\pi f, \quad \lambda f = c$$

Derivation: Relationship Between E and B in a Plane Wave

Starting from Faraday's law, we derive the magnetic field of a plane wave from its electric field.

Step 1: Write E for a plane wave in the z-direction

$$\mathbf{E} = E_0\cos(kz - \omega t)\,\hat{x}$$

Step 2: Apply Faraday's law

$$\nabla \times \mathbf{E} = -\frac{\partial \mathbf{B}}{\partial t}$$

Step 3: Compute the curl of E

$$\nabla \times \mathbf{E} = \frac{\partial E_x}{\partial z}\,\hat{y} = -kE_0\sin(kz - \omega t)\,\hat{y}$$

(Only the $\partial E_x/\partial z$ term survives since $E_x$ depends only on $z$ and $t$.)

Step 4: Integrate to find B

$$-\frac{\partial \mathbf{B}}{\partial t} = -kE_0\sin(kz - \omega t)\,\hat{y}$$

$$\mathbf{B} = -\frac{k}{\omega}E_0\cos(kz - \omega t)\,\hat{y} = \frac{E_0}{c}\cos(kz - \omega t)\,\hat{y}$$

where we used $k/\omega = 1/c$.

Step 5: Identify the key relationships

$$|\mathbf{B}| = \frac{|\mathbf{E}|}{c}, \quad \mathbf{B} = \frac{1}{c}(\hat{k} \times \mathbf{E})$$

$\mathbf{E}$ and $\mathbf{B}$ are perpendicular to each other and to $\hat{k}$, and they oscillate in phase.

Step 6: Verify with Ampere-Maxwell law

$$\nabla \times \mathbf{B} = \frac{\partial B_y}{\partial z}\,(-\hat{x}) = \frac{k}{c}E_0\sin(kz-\omega t)\,(-\hat{x})$$

Wait -- let us be careful with the curl components:

$$(\nabla \times \mathbf{B})_x = -\frac{\partial B_y}{\partial z} = \frac{k}{c}E_0\sin(kz-\omega t)$$

$$\mu_0\epsilon_0\frac{\partial E_x}{\partial t} = \frac{1}{c^2}\omega E_0\sin(kz-\omega t) = \frac{k}{c}E_0\sin(kz-\omega t) \;\checkmark$$

11.2 Energy & Intensity

For a plane wave the energy densities in E and B are equal:

$$u = \epsilon_0 E^2 = \frac{B^2}{\mu_0}$$

The time-averaged intensity (irradiance) is:

$$I = \langle S \rangle = \frac{1}{2}\frac{E_0^2}{\mu_0 c} = \frac{c\epsilon_0 E_0^2}{2} \qquad [\text{W/m}^2]$$

11.2.1 Radiation Pressure

When an EM wave is absorbed by a surface, it exerts a radiation pressure:

$$P_{\rm rad} = \frac{I}{c} \quad \text{(absorbed)}, \qquad P_{\rm rad} = \frac{2I}{c} \quad \text{(reflected)}$$

Derivation: Energy and Momentum of EM Waves

Starting from the energy density and Poynting vector for electromagnetic fields.

Step 1: Write the electromagnetic energy density

$$u = \frac{1}{2}\left(\epsilon_0 E^2 + \frac{B^2}{\mu_0}\right)$$

Step 2: Substitute the plane wave fields

For $E = E_0\cos(kz-\omega t)$ and $B = E_0/c\cdot\cos(kz-\omega t)$:

$$u = \frac{1}{2}\epsilon_0 E_0^2\cos^2(kz-\omega t) + \frac{E_0^2}{2\mu_0 c^2}\cos^2(kz-\omega t)$$

Step 3: Show electric and magnetic energy densities are equal

Since $c^2 = 1/(\mu_0\epsilon_0)$, we have $1/(\mu_0 c^2) = \epsilon_0$, so:

$$u_E = \frac{1}{2}\epsilon_0 E_0^2\cos^2(kz-\omega t) = u_B$$

$$u = \epsilon_0 E_0^2\cos^2(kz-\omega t)$$

Step 4: Compute the Poynting vector

$$\mathbf{S} = \frac{1}{\mu_0}\mathbf{E} \times \mathbf{B} = \frac{1}{\mu_0}E_0\cos(kz-\omega t)\,\hat{x} \times \frac{E_0}{c}\cos(kz-\omega t)\,\hat{y}$$

$$\mathbf{S} = \frac{E_0^2}{\mu_0 c}\cos^2(kz - \omega t)\,\hat{z}$$

Step 5: Time-average the Poynting vector

Using $\langle\cos^2\rangle = 1/2$:

$$\langle\mathbf{S}\rangle = \frac{E_0^2}{2\mu_0 c}\,\hat{z} = \frac{1}{2}\epsilon_0 c E_0^2\,\hat{z}$$

The intensity (time-averaged power per unit area) is $I = |\langle\mathbf{S}\rangle| = E_0^2/(2\mu_0 c)$.

Step 6: Electromagnetic momentum density

$$\mathbf{g} = \mu_0\epsilon_0\mathbf{S} = \frac{\mathbf{S}}{c^2}$$

The momentum carried per unit area per unit time is $\mathbf{S}/c$.

Step 7: Derive radiation pressure for absorption

When a wave is fully absorbed, all its momentum $\Delta p = S\Delta t\,A/c^2 \cdot c = S\,A\,\Delta t/c$ is transferred:

$$P_{\rm rad} = \frac{F}{A} = \frac{\Delta p}{A\,\Delta t} = \frac{\langle S \rangle}{c} = \frac{I}{c}$$

For perfect reflection, the momentum reversal doubles the force: $P_{\rm rad} = 2I/c$.

11.3 Polarization

The polarization state of a plane wave is described by the direction of the electric field vector:

Linear

$\mathbf{E} = E_0\cos(kz-\omega t)\hat{x}$

E oscillates in a fixed plane.

Circular

$\mathbf{E} = E_0[\cos(kz-\omega t)\hat{x} \pm \sin(kz-\omega t)\hat{y}]$

E rotates at constant amplitude; LCP/RCP.

Elliptical

$\mathbf{E} = E_x\hat{x} + E_y e^{i\delta}\hat{y}$

General case; linear and circular are special cases.

Any polarization state can be decomposed into two orthogonal linear polarizations or two circular polarizations. Sunlight is unpolarized (random superposition of all polarization states).

Derivation: Polarization States and Jones Vector Formalism

Starting from the general transverse electric field of a plane wave propagating in $\hat{z}$.

Step 1: Write the most general transverse E field

$$\tilde{\mathbf{E}} = \left(\tilde{E}_{0x}\,\hat{x} + \tilde{E}_{0y}\,\hat{y}\right)e^{i(kz - \omega t)}$$

where $\tilde{E}_{0x} = E_{0x}e^{i\phi_x}$ and $\tilde{E}_{0y} = E_{0y}e^{i\phi_y}$ are complex amplitudes.

Step 2: Define the Jones vector

The polarization state is fully characterized by the Jones vector (ignoring the common propagation factor):

$$\mathbf{J} = \begin{pmatrix} \tilde{E}_{0x} \\ \tilde{E}_{0y} \end{pmatrix} = \begin{pmatrix} E_{0x}e^{i\phi_x} \\ E_{0y}e^{i\phi_y} \end{pmatrix}$$

Step 3: Linear polarization

When $\phi_x = \phi_y$ (or differ by $\pi$), the field oscillates along a fixed direction. Setting $\phi_x = 0$:

$$\mathbf{J}_{\rm linear} = \begin{pmatrix} \cos\alpha \\ \sin\alpha \end{pmatrix}$$

where $\alpha$ is the polarization angle. Examples: $\hat{x}$-polarized $\to \begin{pmatrix}1\\0\end{pmatrix}$, $\hat{y}$-polarized $\to \begin{pmatrix}0\\1\end{pmatrix}$.

Step 4: Circular polarization

Set $E_{0x} = E_{0y} = E_0/\sqrt{2}$ and $\delta = \phi_y - \phi_x = \pm\pi/2$:

$$\mathbf{J}_{\rm RCP} = \frac{1}{\sqrt{2}}\begin{pmatrix} 1 \\ -i \end{pmatrix}, \qquad \mathbf{J}_{\rm LCP} = \frac{1}{\sqrt{2}}\begin{pmatrix} 1 \\ +i \end{pmatrix}$$

The real fields are $\mathbf{E} = E_0[\cos(kz-\omega t)\,\hat{x} \mp \sin(kz-\omega t)\,\hat{y}]$. The tip of $\mathbf{E}$ traces a circle.

Step 5: Elliptical polarization (general case)

For arbitrary $E_{0x}$, $E_{0y}$, and relative phase $\delta = \phi_y - \phi_x$:

$$\mathbf{J}_{\rm elliptical} = \begin{pmatrix} E_{0x} \\ E_{0y}e^{i\delta} \end{pmatrix}$$

The tip of $\mathbf{E}$ traces an ellipse. Eliminate $t$ from the two components to get the polarization ellipse equation:

$$\frac{E_x^2}{E_{0x}^2} + \frac{E_y^2}{E_{0y}^2} - \frac{2E_x E_y}{E_{0x}E_{0y}}\cos\delta = \sin^2\delta$$

Step 6: Special cases recovered

$\delta = 0$ or $\pi$: ellipse degenerates to a line (linear polarization).

$\delta = \pm\pi/2$ and $E_{0x} = E_{0y}$: ellipse becomes a circle (circular polarization).

Any polarization can be decomposed: $\mathbf{J} = c_+\mathbf{J}_{\rm RCP} + c_-\mathbf{J}_{\rm LCP}$.

Simulation: EM Plane Wave Visualization

EM Waves in Vacuum

Visualizes E and B fields of a plane wave, Poynting vector, intensity, and all three polarization types.

Click Run to execute the Python code

First run will download Python environment (~15MB)

Video Lectures & Demonstrations

MIT 8.02 — Electromagnetic waves in vacuum: derivation from Maxwell's equations, polarization, and energy transport.

Comprehensive visualization of linear, circular, and elliptical polarization with Jones vector formalism.

Fortran Implementation

Plane wave propagation in vacuum — computes E and B field components, verifies transversality, and calculates the time-averaged Poynting vector.

EM Plane Wave in Vacuum

Fortran

Computes E, B and Poynting vector fields for a plane wave and verifies energy relations

em_plane_wave.f9046 lines

Click Run to execute the Fortran code

Code will be compiled with gfortran and executed on the server

Griffiths Problem Solutions

Video walkthroughs of Griffiths problems on capacitors, energy storage, and fields — foundational for understanding wave propagation.

Problem 2.28

Problem 2.29

Problem 2.30

Problem 2.31

Problem 2.32

Problem 2.33

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